Mountain glaciations provide an invaluable record for past and present climate change. They are vital for any palaeoclimatologic interpretation and many related research questions. The utilization of this potential is, however, not trivial because of the wide diversity of formerly and currently glaciated mountain ranges. Apart from their specific complex and interacting geomorphological process-systems different climatic and glaciological conditions cause any subsequent global or intra-hemispheric correlations to become incredible challenging. This problem is further enhanced by ongoing specialisation within the scientific community. Working groups primarily focusing on either individual aspects of related research or selected mountain regions often remain somewhat disconnected. As a consequence of the challenges imposed on mountain glaciations, they occasionally seem to become sidelined in the context of Quaternary environmental reconstructions in comparison with other formerly glaciated regions. This discrepancy constitutes an unfortunate and unsatisfactory consequence that should be conquered.

The primary aim of this session is to evaluate the potential of mountain glaciations records and stimulate further research in this important field of research. Contributions on all relevant aspects of the topic are welcomed, for example: (a) glacial landforms and reconstruction of past glaciers, (b) dating techniques and geochronology compilations, (c) glacier dynamics and palaeoclimatic interpretations, or (d) impacts of ecosystems and human evolution/society. Submissions targeting these connections are specifically encouraged. While we encourage submitting abstracts from all abovementioned topics within the broad field of mountain glaciations, we would like to invite in particular those highlighting the specific conditions of mountain glaciations or addressing the relationship and connections between different of their aspects. To address the diversity of mountain glaciations, contributions from high-, middle-, and low-latitude mountain ranges as well as from continental to maritime regions are all welcomed. The time scale of the session will cover the whole time range from Early Pleistocene glaciations to the LGM and Holocene/modern glaciers.

During the past years, precursors of this session have steadily become more popular and attracted contributions from a wide range of research topics and study areas, both with a high diversity of methodological approaches. Their common target was to allow a better understanding of how glacial landforms should be interpreted in a (palaeo)climatic and/or chronological context. The session ultimately aims to facilitate a closer connection between different topological, methodological, and regional working groups related to various aspects of mountain glaciations in space and time. It is further designed to give everyone interested in the emerging collaborative research network “The Legacy of Mountain Glaciations” an opportunity to meet and exchange ideas and expertise.

Please note that the session conveners organized a public splinter meeting on Tuesday (April 9th) between 12.45 and 13.45 in room 0.51 (SMP 6) to meet all colleagues involved with the new application for a COST Action “Legacy of Mountain Glaciations” and those interested in the topic, We will use the opportunity to make this initiative more public and to discuss possible future directions.